石油物探
石油物探
석유물탐
GEOPHYSICAL PROSPECTING FOR PETROLEUM
2009年
6期
557-562
,共6页
碳酸盐岩溶洞%溶洞宽度%数值模拟%物理模拟%"串珠状"反射特征
碳痠鹽巖溶洞%溶洞寬度%數值模擬%物理模擬%"串珠狀"反射特徵
탄산염암용동%용동관도%수치모의%물리모의%"천주상"반사특정
carbonate cavern%cave width%numerical simulation%physical modeling%"string"reflection characteristic
为了模拟碳酸盐岩储层中不同横向尺度溶洞的地震响应特征,设计了具有不同横向尺度但高度和充填物相同的溶洞地质模型,分别采用数值模拟技术和物理模拟技术进行了正演模拟,分析研究了由溶洞宽度变化引起的地震响应变化的特征.研究结果表明,溶洞宽度的变化会引起溶洞反射特征"串珠"中"珠"的数目发生改变,溶洞顶、底位置与溶洞绕射波的相位有对应关系,在偏移剖面中"串珠"尺度与实际溶洞尺度之间存在较大差异.对比同一模型的数值模拟和物理模拟正演结果发现,所得的不同横向尺度溶洞的地震响应特征总的趋势是一致的,但在细节上有所差异,这表明两种正演方法具有互补性,为研究溶洞的"串珠状"地震波反射特征提供了更好的手段.
為瞭模擬碳痠鹽巖儲層中不同橫嚮呎度溶洞的地震響應特徵,設計瞭具有不同橫嚮呎度但高度和充填物相同的溶洞地質模型,分彆採用數值模擬技術和物理模擬技術進行瞭正縯模擬,分析研究瞭由溶洞寬度變化引起的地震響應變化的特徵.研究結果錶明,溶洞寬度的變化會引起溶洞反射特徵"串珠"中"珠"的數目髮生改變,溶洞頂、底位置與溶洞繞射波的相位有對應關繫,在偏移剖麵中"串珠"呎度與實際溶洞呎度之間存在較大差異.對比同一模型的數值模擬和物理模擬正縯結果髮現,所得的不同橫嚮呎度溶洞的地震響應特徵總的趨勢是一緻的,但在細節上有所差異,這錶明兩種正縯方法具有互補性,為研究溶洞的"串珠狀"地震波反射特徵提供瞭更好的手段.
위료모의탄산염암저층중불동횡향척도용동적지진향응특정,설계료구유불동횡향척도단고도화충전물상동적용동지질모형,분별채용수치모의기술화물리모의기술진행료정연모의,분석연구료유용동관도변화인기적지진향응변화적특정.연구결과표명,용동관도적변화회인기용동반사특정"천주"중"주"적수목발생개변,용동정、저위치여용동요사파적상위유대응관계,재편이부면중"천주"척도여실제용동척도지간존재교대차이.대비동일모형적수치모의화물리모의정연결과발현,소득적불동횡향척도용동적지진향응특정총적추세시일치적,단재세절상유소차이,저표명량충정연방법구유호보성,위연구용동적"천주상"지진파반사특정제공료경호적수단.
In order to simulate the seismic responses of caverns with different lateral scale in carbonate reservoirs,we designed cavern geologic models with same height and fillings but different lateral scale,adopted numerical simulation and physical modeling for forward simulation,and analyzed the variation features of seismic responses via the changes of cave width.The results indicate that the changes of cave width will cause the number of"pill"varying in the"string"reflection characteristic,the top and bottom of cave has corresponding relationship with cave diffracted wave.On migration section,the scale of"string"has large contrast with actual cave width.The comparison on forward simulation results of the same model by numerical simulation and physical modeling methods shows that the overall trend of seismic response of different lateral-scale caverns is uniform,but difference exists in detail,which indicates that the two methods are complementary and provides better means for study the"string"reflection characteristic of caverns.